塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

沈卫兵; 庞雄奇; 陈践发; 王阳洋; 张科; 高兆富; 贾颖超; 陈泽亚

doi:10.14027/j.issn.1000-0550.2018.101

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塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

沈卫兵, 庞雄奇, 陈践发, 王阳洋, 张科, 高兆富, 贾颖超, 陈泽亚

文章导航 > 沉积学报 > 2018 > 36(5): 1008-1022

沈卫兵, 庞雄奇, 陈践发, 王阳洋, 张科, 高兆富, 贾颖超, 陈泽亚. 塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式[J]. 沉积学报, 2018, 36(5): 1008-1022. doi: 10.14027/j.issn.1000-0550.2018.101

引用本文:

SHEN WeiBing, PANG XiongQi, CHEN JianFa, WANG YangYang, ZHANG Ke, GAO ZhaoFu, JIA YingChao, CHEN ZeYa. Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2018, 36(5): 1008-1022. doi: 10.14027/j.issn.1000-0550.2018.101

Citation:

SHEN WeiBing, PANG XiongQi, CHEN JianFa, WANG YangYang, ZHANG Ke, GAO ZhaoFu, JIA YingChao, CHEN ZeYa. Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2018, 36(5): 1008-1022. doi: 10.14027/j.issn.1000-0550.2018.101

引用本文:

Citation:

SHEN WeiBing, PANG XiongQi, CHEN JianFa, WANG YangYang, ZHANG Ke, GAO ZhaoFu, JIA YingChao, CHEN ZeYa. Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2018, 36(5): 1008-1022. doi: 10.14027/j.issn.1000-0550.2018.101

塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

1.
中国地质科学院地质研究所, 自然资源部深地动力学重点实验室, 北京 100037;
2.
中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249;
3.
中国石油塔里木油田分公司勘探开发研究院, 新疆库尔勒 841000;
4.
中国石油华北油田分公司勘探开发研究院, 河北任丘 062550

基金项目: 国家自然科学基金项目（41703017）；中国地质科学院地质研究所基本科研业务费项目（J1717）；国家重点基础研究发展计划（973计划）项目（2011CB201100）

详细信息

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

中图分类号: P618.13

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Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

1.
Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China;
3.
Research Institute of Exploration and Development, PetroChina Tarim Oilfield, Korla, Xinjiang 841000, China;
4.
Research Institute of Exploration and Development, PetroChina Huabei Oilfield, Renqiu, Hebei 062550, China

Funds: National Natural Science Foundation of China, No.41703017; Basic Scientific Research Operating Expense Program from Institute of Geology, Chinese Academy of Geological Sciences,No.J1717; National Basic Research Program of China (973 Program), No.2011CB201100

摘要

摘要: 从多元地质条件及其空间匹配关系角度出发，综合地质剖析及地球化学示踪等方法，对塔里木盆地塔中隆起奥陶系油气输导体系、运移方向及分布特征等进行的精细研究。结果显示：断裂、源储接触关系及盖层等共同控制着油气垂向运移的距离及层位；构造背景、不整合面、渗透性输导层、断裂的配置关系等控制着油气侧向运移的方向、通道和距离；海平面升降旋回、优质储层的配置关系控制着油气垂向聚集层位及平面分布规律。进一步结合研究区烃源岩条件、储层类型等研究成果，基于源储纵向接触关系及油气垂向运移距离，目的层油气成藏模式可分为近源混合成藏模式与远源混合成藏模式；根据油气来源区域及油气横向运移距离，又可分为内部源岩叠加混合成藏模式与内外部源岩交叉混合成藏模式。
- 碳酸盐岩 /
- 输导体系 /
- 主控因素 /
- 油气成藏 /
- 塔里木盆地
Abstract: In order to further clarify the role of different geological conditions on hydrocarbons accumulation process, the major controlling factors of Ordovician hydrocarbons accumulation in the Tazhong Uplift, Tarim Basin are studied based on the view points of diverse geological conditions and their relationship in space. The results showed that the vertical hydrocarbons migration distance and accumulation layers were controlled by vertical source-reservoir distribution, faults, and caprocks. Structures played a major role in lateral direction of hydrocarbons migration. The lateral migration pathways were governed by unconformities, transport faults, and porous permeable carrier beds. Apart from the excellent reservoir controls, hydrocarbons enrichment was controlled by tectonic events. Based on the analysis of factors mentioned above and coupled with oil sources conditions and excellent reservoirs, two types of hydrocarbon accumulation models could be retained based on the vertical hydrocarbon migration distance, including a multi-sourced area model and a single-sourced area model. In addition, the accumulation models could be also classified into near source accumulation and far source accumulation based on the lateral hydrocarbons migration distance.
- carbonate rock /
- migration pathway /
- key factor /
- hydrocarbon accumulation /
- Tarim Basin

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[1]	岳翀, 赵晓明, 葛家旺, 马畅, 廖晋, 宋鹏, 方小宇, 范廷恩. 琼东南盆地莺歌海组陆架边缘轨迹演化及主控因素 . 沉积学报, 2023, 41(1): 110-125. doi: 10.14027/j.issn.1000-0550.2022.065
[2]	王文博, 傅恒, 闾廖然, 朱梦琦, 陈康, 张智南, 刘鑫北, 熊锐, 王荣刚, 周杨. 塔里木盆地顺北地区奥陶系碳酸盐岩层序模式及其意义 . 沉积学报, 2021, 39(6): 1451-1465. doi: 10.14027/j.issn.1000-0550.2021.078
[3]	李继岩. 多期构造裂缝发育充填特征及其主控因素——以济阳坳陷平南潜山为例 . 沉积学报, 2020, 38(2): 420-428. doi: 10.14027/j.issn.1000-0550.2019.117
[4]	孙东, 潘建国, 胡再元, 杨丽莎, 周俊峰, 韩杰, 李闯, 房启飞. 塔里木盆地塔中Ⅲ区奥陶系碳酸盐岩油气成藏主控因素及有利区带 . 沉积学报, 2019, 37(4): 868-877. doi: 10.14027/j.issn.1000-0550.2018.176
[5]	杨伟利, 王毅, 张众琛, 梁晨, 李京昌. 塔里木盆地顺南地区中-下奥陶统正演沉积数值模拟 . 沉积学报, 2017, 35(1): 117-123. doi: 10.14027/j.cnki.cjxb.2017.01.012
[6]	孙辉, 刘少治, 马宏霞, 鲁银涛, 许小勇. 东非鲁武马盆地海底水道—朵体体系粗粒浊流沉积物波特征及主控因素 . 沉积学报, 2017, 35(4): 763-771. doi: 10.14027/j.cnki.cjxb.2017.04.010
[7]	韩杰, 吴萧, 潘文庆, 江杰, 张敏. 塔里木盆地西北缘巴楚—乌什露头区奥陶系沉积相特征 . 沉积学报, 2015, 33(4): 764-772. doi: 10.14027/j.cnki.cjxb.2015.04.015
[8]	付红军. 海塔盆地中部主要断陷带早期和晚期油气富集的主控因素 . 沉积学报, 2014, 32(5): 981-987.
[9]	. 塔里木盆地奥陶系碳酸盐岩颗粒滩沉积组合及展布特征 . 沉积学报, 2014, 32(3): 418-428.
[10]	. 滨里海盆地碳酸盐岩高频层序特征及其油气勘探应用——以M区块石炭系KT—I含油层系为例 . 沉积学报, 2013, 31(04): 608-615.
[11]	倪新锋. 塔里木盆地英买力—哈拉哈塘地区奥陶系碳酸盐岩岩溶型储层特征及成因 . 沉积学报, 2011, 29(3): 465-474.
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[13]	王圣柱. 东营凹陷南斜坡深层成藏特征及主控因素分析 . 沉积学报, 2007, 25(3): 474-481.
[14]	陈景山. 塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布 . 沉积学报, 2007, 25(6): 858-868.
[15]	李平平邹华耀郝芳. 准噶尔盆地腹部侏罗系顶部风化壳的发育机制及其油气成藏效应 . 沉积学报, 2006, 24(06): 889-896.
[16]	马达德, 寿建峰, 胡勇, 王少依, 徐宁. 柴达木盆地柴西南区碎屑岩储层形成的主控因素分析 . 沉积学报, 2005, 23(4): 589-595.
[17]	李慧莉, 邱楠生, 金之钧, 吕修祥. 塔里木盆地克拉2气田储层流体包裹体与油气成藏研究 . 沉积学报, 2003, 21(4): 648-653.
[18]	岳伏生, 马龙, 李天顺. 查干凹陷下白垩统碎屑岩储层成岩演化与油气成藏 . 沉积学报, 2002, 20(4): 644-649.
[19]	刘洛夫, 赵建章, 张水昌, 方家虎, 肖中尧. 塔里木盆地志留系沥青砂岩的形成期次及演化 . 沉积学报, 2000, 18(3): 475-479.
[20]	徐志强, 陈永武, 熊明. 影响深层碎屑岩次生孔隙发育的因素——冀中坳陷与塔里木盆地实例讨论 . 沉积学报, 1997, 15(S1): 102-105.

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塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

1. 中国地质科学院地质研究所, 自然资源部深地动力学重点实验室, 北京 100037;

2. 中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249;

3. 中国石油塔里木油田分公司勘探开发研究院, 新疆库尔勒 841000;

4. 中国石油华北油田分公司勘探开发研究院, 河北任丘 062550

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

收稿日期: 2017-11-06
修回日期: 2018-01-18
刊出日期: 2018-10-10

中图分类号: P618.13

关键词:

摘要: 从多元地质条件及其空间匹配关系角度出发，综合地质剖析及地球化学示踪等方法，对塔里木盆地塔中隆起奥陶系油气输导体系、运移方向及分布特征等进行的精细研究。结果显示：断裂、源储接触关系及盖层等共同控制着油气垂向运移的距离及层位；构造背景、不整合面、渗透性输导层、断裂的配置关系等控制着油气侧向运移的方向、通道和距离；海平面升降旋回、优质储层的配置关系控制着油气垂向聚集层位及平面分布规律。进一步结合研究区烃源岩条件、储层类型等研究成果，基于源储纵向接触关系及油气垂向运移距离，目的层油气成藏模式可分为近源混合成藏模式与远源混合成藏模式；根据油气来源区域及油气横向运移距离，又可分为内部源岩叠加混合成藏模式与内外部源岩交叉混合成藏模式。

English Abstract

Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

1. Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;

2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China;

3. Research Institute of Exploration and Development, PetroChina Tarim Oilfield, Korla, Xinjiang 841000, China;

4. Research Institute of Exploration and Development, PetroChina Huabei Oilfield, Renqiu, Hebei 062550, China

Received Date: 2017-11-06
Rev Recd Date: 2018-01-18
Publish Date: 2018-10-10

Keywords:

Abstract: In order to further clarify the role of different geological conditions on hydrocarbons accumulation process, the major controlling factors of Ordovician hydrocarbons accumulation in the Tazhong Uplift, Tarim Basin are studied based on the view points of diverse geological conditions and their relationship in space. The results showed that the vertical hydrocarbons migration distance and accumulation layers were controlled by vertical source-reservoir distribution, faults, and caprocks. Structures played a major role in lateral direction of hydrocarbons migration. The lateral migration pathways were governed by unconformities, transport faults, and porous permeable carrier beds. Apart from the excellent reservoir controls, hydrocarbons enrichment was controlled by tectonic events. Based on the analysis of factors mentioned above and coupled with oil sources conditions and excellent reservoirs, two types of hydrocarbon accumulation models could be retained based on the vertical hydrocarbon migration distance, including a multi-sourced area model and a single-sourced area model. In addition, the accumulation models could be also classified into near source accumulation and far source accumulation based on the lateral hydrocarbons migration distance.

引用本文:

Citation:

SHEN WeiBing, PANG XiongQi, CHEN JianFa, WANG YangYang, ZHANG Ke, GAO ZhaoFu, JIA YingChao, CHEN ZeYa. Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China[J]. Acta Sedimentologica Sinica, 2018, 36(5): 1008-1022. doi: 10.14027/j.issn.1000-0550.2018.101

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塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

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Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

计量

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塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

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Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

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塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

作者简介: 沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

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Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

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出版历程

目录

塔里木盆地塔中隆起奥陶系碳酸盐岩油气运聚主控因素及成藏模式

doi: 10.14027/j.issn.1000-0550.2018.101

作者简介: 沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

English Abstract

Accumulation Model based on Factors Controlling Ordovician Hydrocarbons Migration and Enrichment in the Tazhong Uplift, Tarim Basin, NW China

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友情链接

期刊在线

联系我们

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com

作者简介:
沈卫兵,男,1987年出生,博士,碳酸盐岩油气藏形成与分布规律、同位素地球化学,E-mail:swb560316@126.com